Resources from the Ocean: Mineral Resources on the Deep Sea Floor, Energy Resources, Biotic Resources
Geography › Oceanography · Topic 6.12
The oceans supply minerals, energy and living resources. Mineral resources include sand and gravel, petroleum and gas from continental shelves, placer deposits, and on the deep sea floor polymetallic nodules, cobalt-rich crusts and polymetallic sulphides. Energy resources include offshore wind, tidal, wave and ocean thermal energy. Biotic resources include fish, shellfish, seaweed and other marine life. These resources are governed by the law of the sea, and their use has to be balanced against overfishing, pollution and damage to deep-sea ecosystems.
9 min read · UPSC Prelims · Geography · Oceanography
At a Glance
- Deep sea minerals Nodules, crusts, sulphides
- Energy Tidal, wave, thermal, offshore wind
- Biotic Fish, shellfish, seaweed
- Seabed authority International Seabed Authority
- Policy theme Blue economy
- Exam link UPSC Prelims, Geography: Oceanography
Where Does It Fit?
This topic follows the major currents and the account of the ocean basins, and turns to what people take from the sea. It leads into the Deep Ocean Mission of India and the law of the sea that governs these resources. Previous topic: Atlantic Meridional Overturning Circulation (AMOC). Next topic: Deep Ocean Mission.
What Are Ocean Deposits?
In short: the sea floor is covered by sediment that comes from the land, from dead sea life, and from chemical processes in the water.
| Type | Source | Where found |
|---|---|---|
| Terrigenous deposits | Rock fragments carried from the land by rivers, wind and glaciers: sand, silt, mud | Continental shelf and slope, deltas; also the Bengal Fan |
| Calcareous ooze | Shells of tiny animals and plants such as foraminifera and coccolithophores, mainly calcium carbonate | Warm, shallower open ocean floors, above about 4,000 to 5,000 m |
| Siliceous ooze | Remains of diatoms and radiolaria, mainly silica | Cold, productive waters of the Southern Ocean and the North Pacific, and the equatorial Pacific |
| Red clay | Fine windblown dust and volcanic ash, red from iron oxide | Deepest ocean basins, where calcium carbonate dissolves below the carbonate compensation depth; the slowest to accumulate |
| Authigenic (hydrogenous) deposits | Chemical precipitation from sea water: manganese nodules, phosphorites, glauconite | Abyssal plains, shelves with slow deposition |
| Volcanic and cosmogenic deposits | Ash and lava; extraterrestrial dust and microscopic meteorites | Near volcanic arcs and ridges; everywhere in small amounts |
The sediments are a record of the history of the Earth. Cores from the sea floor reveal the climate over millions of years, and the age of the sea floor sediment helped prove sea-floor spreading, as in Convectional Current Theory and Mapping of the Ocean Floor.
What Mineral Resources Does the Ocean Hold?
- Offshore oil and gas: about a third of the world’s oil and gas now comes from the continental shelf, such as the North Sea, the Gulf of Mexico, the Persian Gulf and Bombay High, as in Relief of the Ocean Floor: Continental Shelf, Continental Slope, Deep Sea Plain, Oceanic Deep and Trenches.
- Placer deposits: heavy minerals, including ilmenite, rutile, zircon, monazite and garnet, concentrated by waves and currents on beaches and the shelf. The beach sands of Keralam (Kerala), Tamil Nadu and Odisha are among the richest in the world and are a source of titanium and thorium.
- Polymetallic or manganese nodules: potato-sized lumps on abyssal plains at 4,000 to 6,000 m, formed over millions of years around a core, rich in manganese, nickel, copper and cobalt. The Clarion-Clipperton Zone in the Pacific and the Central Indian Ocean Basin are the main fields.
- Cobalt-rich ferromanganese crusts: layers on the slopes of seamounts, with cobalt, nickel and platinum.
- Polymetallic sulphides: deposits of copper, zinc, gold and silver around hydrothermal vents on mid-oceanic ridges, as in Minor Relief Features: Mid-Oceanic Ridges, Seamounts, Submarine Canyons, Guyots, Atolls.
- Gas hydrates: ice-like solids of methane and water in cold, high-pressure sediments of the slope, a potential energy source. They are found in the Krishna-Godavari and Mahanadi basins and the Andaman area of India, but a method of safe extraction is not yet commercial. Methane is a strong greenhouse gas, so a release would be risky.
- Dissolved minerals and others: common salt, magnesium, bromine, potash, fresh water by desalination, phosphorite nodules and sand and gravel for construction.
Who Governs the Seabed, and What Is India Doing?
The seabed beyond the national jurisdiction is called the Area. Under the United Nations Convention on the Law of the Sea, the Area and its resources are the common heritage of mankind, as in United Nations Convention on the Law of the Sea (UNCLOS). The International Seabed Authority, ISA, based in Kingston, Jamaica, grants exploration contracts and is meant to frame the rules, the mining code, for commercial exploitation. India was an early pioneer investor: it received the first registration as a pioneer investor in 1987, and has an ISA contract of 2002 for polymetallic nodules over 75,000 square kilometres in the Central Indian Ocean Basin, and a 2016 contract for polymetallic sulphides over 10,000 square kilometres on the Central Indian Ridge and the Carlsberg Ridge. India’s Deep Ocean Mission, approved in 2021 with an outlay of about 4,000 crore rupees for five years, includes the development of technology for deep-sea mining and a crewed submersible, Matsya 6000, to go to 6,000 m.
Commercial deep-sea mining has not yet started. The ISA council’s talks in March 2026 ended without an agreed mining code, and more than 30 countries have called for a pause or a moratorium, because the effects on deep-sea ecosystems are poorly known. Meanwhile, the United States has opened its own domestic permitting route for companies, which many countries see as outside the UNCLOS system, and the status of the first application is still unsettled. As an analytical point, the debate sets the demand for nickel, cobalt and copper, needed for batteries and the energy transition, against the risk to some of the least-known habitats on Earth, and the recycling of metals and the technologies that use less cobalt can reduce the pressure.
What Energy Can the Oceans Provide?
| Source | How it works | Status and India |
|---|---|---|
| Offshore oil and gas | Drilling on the continental shelf and in deep water | About a third of world oil production; Bombay High is India’s largest offshore field, and the Krishna-Godavari basin has deep-water gas |
| Offshore wind | Turbines at sea, where winds are stronger and steadier than on land | Fast growing in Europe and China; India has a coastline suited to it off Gujarat and Tamil Nadu, with a national policy since 2015 and support for the first projects approved in 2024 |
| Tidal energy | Turbines driven by the rise and fall of the tide, as in Tides: Tidal Currents, Types and Importance | Predictable, but limited to sites with a high tidal range |
| Wave energy | Machines that convert the up-and-down motion of surface waves to electricity | Still at the pilot stage; an Indian pilot was tested off Vizhinjam in Keralam |
| otec/" class="maargx-auto-link" data-preview="At a Glance Needs About 20 C temperature gap Cycles Closed, open, hybrid Suitable zone Tropical seas Power type Continuous base load…">Ocean thermal energy conversion (OTEC) | Uses the difference in temperature of at least about 20 degrees Celsius between warm surface water and cold deep water to run a turbine | Suited for tropical islands, as in Temperature of Ocean Water: Vertical and Spatial Variations, the Thermocline; India’s NIOT built a low-temperature thermal desalination plant at Kavaratti in Lakshadweep |
| Salinity gradient and currents | Energy from the difference between fresh and salt water, or from strong currents | Experimental |
| Gas hydrates | Methane trapped in sediments of the slope | Large resources in India’s Krishna-Godavari, Mahanadi and Andaman areas; extraction is not yet commercial |
What Are the Biotic Resources of the Ocean?
- Fisheries: the oceans give about 80 million tonnes of wild-caught fish and other seafood a year, and aquaculture now supplies about as much again. The best fishing grounds are on the continental shelf, where warm and cold currents meet and upwelling brings nutrients: the Northwest Pacific, the Northeast Atlantic, the Peruvian coast and the Indian Ocean. India is the second largest fish producer in the world, with a coastline of over 7,500 km, after China.
- Seaweed: used for food, agar and alginates, fertiliser and biofuel; India is promoting seaweed farming along the coast of Tamil Nadu, Gujarat and Lakshadweep, and has set up a multipurpose seaweed park at Ramanathapuram.
- Shellfish, pearls and corals: oysters, prawns, mussels and pearls, such as at Tuticorin in the Gulf of Mannar.
- Marine biotechnology: sponges, corals, and microbes provide compounds for medicines, such as anticancer drugs.
- Mangroves and coastal ecosystems: nurseries of fish, protectors of coasts and stores of carbon, as in the Sundarbans.
How Sustainable Is the Use of Ocean Resources?
The FAO estimates that more than a third of the world’s marine fish stocks are fished beyond sustainable limits, and the share has been rising for decades. Overfishing, destructive methods such as bottom trawling, bycatch, subsidies that support the overcapacity of fleets, illegal fishing, pollution and warming of the sea are the key causes, as in Temperature of Ocean Water: Vertical and Spatial Variations, the Thermocline. The collapse of the cod fishery at the Grand Banks in 1992 is a standard example, as in Major Ocean Currents of the World and Their Effects.
The concept of the blue economy, the sustainable use of ocean resources for growth, jobs and ocean health, is the response. Instruments include catch limits, closed seasons such as the annual fishing ban of 61 days in Indian waters, marine protected areas, the global target to protect 30 per cent of the oceans by 2030 under the Kunming-Montreal Global Biodiversity Framework, and the new treaty on the biodiversity of the high seas, the BBNJ Agreement, which was due to come into force in January 2026 after reaching the 60 ratifications needed. India’s policies include the Pradhan Mantri Matsya Sampada Yojana, launched in 2020 to raise fish production and to modernise the sector, and the Deep Ocean Mission. As an analytical point, small-scale fishers, who are the majority of Indian fishers, depend on the nearshore stocks that are under the most pressure, so the sector needs better data, credit and cold storage as much as it needs regulation.
Why Is This Topic Important?
- Concepts OTEC and blue economy asked
- India Fisheries and offshore wind
- Sustainability Overfishing and treaties
What Came Next?
The next topic describes India’s Deep Ocean Mission. Next topic: Deep Ocean Mission.
Key People and Terms
- OTEC Energy from ocean temperature difference
- Offshore wind Wind farm at sea
- Overfishing Catching fish faster than they reproduce
- Bycatch Unwanted catch of other species
- Blue economy Sustainable use of ocean resources
- BBNJ Biodiversity Beyond National Jurisdiction agreement
Exam Corner
Points to Remember
- OTEC needs about 20 degrees Celsius difference.
- India’s annual fishing ban is 61 days.
- More than a third of stocks are overfished.
- 30 by 30 is the ocean protection target.
- PMMSY was launched in 2020.
Do Not Confuse With
- Tidal and wave energy Tide range versus surface waves
- Capture fishery and aquaculture Wild catch versus farmed fish
- Blue economy and fishing industry Sustainable sector-wide use versus one sector
Memory Hook
Wind, tide, wave and heat power the sea; fish feed us, but only if we leave enough in the water.
Mains Angle
Questions ask for potential and sustainability. These points add depth.
- Energy Offshore wind and OTEC
- Food Fisheries and seaweed
- Governance Blue economy and BBNJ
A Question You May Face
An original practice question, not a past paper question.
“Discuss the energy and biotic resources of the oceans and the challenges of using them sustainably, with reference to India’s blue economy.”
How to Answer
- Energy Forms and status.
- Biotic Fish and seaweed.
- Problems Overfishing and warming.
- Policy Blue economy and treaties.
GS Relevance
Frequently Asked Questions
What are polymetallic nodules?
Polymetallic nodules are potato-sized lumps of manganese, iron, nickel, copper and cobalt that form very slowly on the deep abyssal plains, around a small core such as a shark tooth. The Clarion-Clipperton Zone in the Pacific and the Central Indian Ocean Basin have large fields.
What are placer deposits?
Placer deposits are concentrations of heavy and valuable minerals, such as ilmenite, rutile, zircon and monazite, separated from sand by waves and currents. The beaches of Keralam, Tamil Nadu and Odisha have rich placer deposits, used for titanium, thorium and other materials.
What is the International Seabed Authority?
The International Seabed Authority is an organisation set up under the UN Convention on the Law of the Sea, located in Kingston, Jamaica. It organises and controls activities in the international seabed area, which is the common heritage of mankind, and it grants exploration contracts and is developing mining rules.
What is ocean thermal energy conversion?
Ocean thermal energy conversion, OTEC, produces electricity using the temperature difference of at least about 20 degrees Celsius between warm surface water and cold deep water. It is suited for tropical areas with deep water close to the coast, such as islands, and can also provide fresh water by desalination.
What is overfishing?
Overfishing is catching fish faster than the stocks can reproduce, leading to decline or collapse of the population. According to the FAO, more than a third of the world's marine fish stocks are overfished, and the collapse of the Grand Banks cod fishery in 1992 is a well-known example.
PYQ Practice — Statement Analysis
1 Red clay is found in the deepest parts of the ocean.
Calcium carbonate dissolves below the compensation depth.
2 Biogenic oozes are formed from the remains of land rocks.
They come from marine organisms.
3 OTEC works on the temperature difference between surface and deep ocean water.
A difference of about 20 degrees Celsius is needed.
4 Cold-water fish stocks have never been overfished.
The Grand Banks cod collapsed in 1992.
Past Mains Questions on This Topic
This topic comes under Oceanography. UPSC Mains questions asked on the matching syllabus topic, year-wise with marks:
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